Chromite from the Blue Ridge province of North Carolina.

American Journal of Science


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Chromite is found as ubiquitous accessory grains and occasional segregations within dunite bodies. Results of analysis of chromite textures and chemistry and estimation of equilibration T of olivine-chromite pairs are cited as evidence that the dunites are metamorphic rocks rather than primary mantle peridotites. They are considered to be disrupted fragments of ophiolites that were emplaced before or during the peak of Ordovician metamorphism which was responsible for dehydration of serpentine-bearing rocks and alteration of chromite compositions and textures.-M.S.
Publication type Article
Publication Subtype Journal Article
Title Chromite from the Blue Ridge province of North Carolina.
Series title American Journal of Science
Volume 284
Issue 4-5
Year Published 1984
Language English
Contributing office(s) Eastern Mineral and Environmental Resources Science Center
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title American Journal of Science
First page 507
Last page 529
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